|km mi 130 81 120 75 110 68 Thermasphere 100 62 90 56 Makopause 80 50 70 43 Mesosphere 60 3기 Stratopause 50 31 40 25 30 Stratosphere 19 20 12 Tropopaus 10 Tropophere -100 -80 -60 -40 -20 20 40 60 Matching Layers Deseriptions A. The layer of the atmosphere in which all weather phenomena occur. B. The layers of the atmosphere where the temperature is increasing with altitude. C. The layer of the atmosphere in which ozone is produced. D. The layer of the atmosphere which contains the lonosphere. E. The layers of the atmosphere where the temperature is decreasing with altitude. F. The layer of the atmosphere where the heterosphere begins.
|km mi 130 81 120 75 110 68 Thermasphere 100 62 90 56 Makopause 80 50 70 43 Mesosphere 60 3기 Stratopause 50 31 40 25 30 Stratosphere 19 20 12 Tropopaus 10 Tropophere -100 -80 -60 -40 -20 20 40 60 Matching Layers Deseriptions A. The layer of the atmosphere in which all weather phenomena occur. B. The layers of the atmosphere where the temperature is increasing with altitude. C. The layer of the atmosphere in which ozone is produced. D. The layer of the atmosphere which contains the lonosphere. E. The layers of the atmosphere where the temperature is decreasing with altitude. F. The layer of the atmosphere where the heterosphere begins.
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Question
Transcribed Image Text:|km
mi
|130
81
120
75
110
68
Thermasphere
100
62
90
56
Makopause
80
50
70
43
Mesosphere
60
3기
Stratopause
50
31
40
25
Stratosphere
30
19
20
12
Tropopause
10
6
Tropophere
-100 -80 -60 -40 -20
20
40
60
Matching Layers Deseriptions
A. The layer of the atmosphere in which all weather phenomena occur.
B. The layers of the atmosphere where the temperature is increasing with altitude.
C. The layer of the atmosphere in which ozone is produced.
D. The layer of the atmosphere which contains the lonosphere.
E. The layers of the atmosphere where the temperature is decreasing with altitude.
F. The layer of the atmosphere where the heterosphere begins.
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